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History of Phoenicia by George Rawlinson
page 25 of 539 (04%)
rise jagged precipices of white limestone, crowned far overhead by many
a convent and village.[156] The course of the Nahr-el-Kelbis about equal
to that of the Adonis.

The Damour or Tamyras drains the western flank of Lebanon to the south
of Jebel Sunnin (about Lat. 33º 45´), the districts known as Menassif
and Jourd Arkoub, about Barouk and Deir-el-Kamar. It collects the waters
from an area of about 110 square miles, and carries them to the sea in
a course which is a little north of west, reaching it half-way between
Khan Khulda (Heldua) and Nebbi Younas. The scenery along its banks is
tame compared with that of the more northern rivers.

The Nahr-el-Auly or Bostrenus rises from a source to the north-east of
Barouk, and flows in a nearly straight course to the south-west for a
distance of nearly thirty-five miles, when it is joined by a stream
from Jezzin, which flows into it from the south-east. On receiving this
stream, the Auly turns almost at a right angle, and flows to the west
down the fine alluvial track called Merj Bisry, passing from this point
through comparatively low ground, and between swelling hills, until it
reaches the sea two miles to the north of Sidon. Its entire course is
not less than sixty miles.

The Zaherany repeats on a smaller scale the course of the Bostrenus. It
rises near Jerjû'a from the western flank of Jebel Rihan, the southern
extremity of the Lebanon range, and flows at first to the south-west.
The source is "a fine large fountain bursting forth with violence, and
with water enough for a mill race."[157] From this the river flows in
a deep valley, brawling and foaming along its course, through tracts of
green grass shaded by black walnut-trees for a distance of about five
miles, after which, just opposite Jerjû'a, it breaks through one of the
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